Rock Identifier
Tumbled yellow-brown stone, likely quartzite or chalcedony (Quartz-rich rock; predominantly microcrystalline quartz (SiO₂), identification uncertain from image alone) — metamorphic
metamorphic

Tumbled yellow-brown stone, likely quartzite or chalcedony

Quartz-rich rock; predominantly microcrystalline quartz (SiO₂), identification uncertain from image alone

AI-generated identification · may be incorrect

Smooth, rounded, opaque to slightly translucent, with yellow-brown coloration likely from iron oxides. Quartz-rich material has Mohs hardness about 6.5–7, vitreous to waxy luster, and no obvious cleavage; specific gravity is typically 2.6–2.7.

Identified More metamorphic
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Physical properties

Smooth, rounded, opaque to slightly translucent, with yellow-brown coloration likely from iron oxides. Quartz-rich material has Mohs hardness about 6.5–7, vitreous to waxy luster, and no obvious cleavage; specific gravity is typically 2.6–2.7.

Formation & geological history

Likely a naturally quartz-rich pebble shaped by water and later tumbled or polished; iron staining produced the ochre color. The source rock may range from Precambrian to younger, depending on locality.

Uses & applications

Used as a decorative or worry stone, lapidary material, and inexpensive collectible; similar material may be used for small carvings or cabochons.

Geological facts

The rounded form and uniform surface indicate abrasion or deliberate tumbling rather than a fresh crystal face. It could also be yellow jasper or iron-stained chert, which cannot be reliably separated visually here.

Field identification & locations

Test hardness against glass or a steel file, inspect translucency at the edges, and use a streak test and specific-gravity measurement for confirmation. Comparable pebbles occur widely in river gravels and commercial rock-tumbling mixes.